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贵州省岩溶洼地地质成因分析
引用本文:高奋飞,刘宏,邓杰文. 贵州省岩溶洼地地质成因分析[J]. 路基工程, 2012, 0(6): 23-26
作者姓名:高奋飞  刘宏  邓杰文
作者单位:1.1贵州大学喀斯特环境与地质灾害防治教育部重点实验室,贵阳 550003
基金项目:贵州省优秀青年科技人才培养专项资金项目
摘    要:通过贵州省岩溶洼地实地考察分析,从地质学角度对岩溶洼地成因做了详细的归纳分析。提出了岩溶洼地地质成因有岩溶裂隙发育形成和地下河流岩溶塌陷形成两种,并对这两种不同成因类型的岩溶洼地地貌特征做了详细对比。

关 键 词:岩溶洼地   地质成因   岩溶裂隙   地下河流
收稿时间:2019-11-06

Analysis on Geological Genesis of Karst Depression in Guizhou Province
GAO Fen-fei,LIU Hong,DENG Jie-wen. Analysis on Geological Genesis of Karst Depression in Guizhou Province[J]. , 2012, 0(6): 23-26
Authors:GAO Fen-fei  LIU Hong  DENG Jie-wen
Affiliation:1(1.Key Laboratory of Karst Environment and Geohazard Prevention(Guizhou University),Ministry of Education, Guiyang 550003,China;2.Xi’an Engineering Investigation and Design Research Institute of China National Non-ferrous Metals Industry,Xi’an 710054,China)
Abstract:Through the field investigation and analysis of karst depression in Guizhou Province,the genesis thereof is generalized and analyzed in details from the viewpoint of geology.The two origins,including karst fissure development and karst collapse along underground river,are proposed and the geomorphic features of the karst depression caused therefrom are compared carefully.
Keywords:karst depression  geological genesis  karst fissure  underground river
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